• 全国中文核心期刊
  • 中国科技核心期刊
  • 美国工程索引(EI)收录期刊
  • Scopus数据库收录期刊
NIU Geng, SUN De-an, WEI Chang-fu, YAN Rong-tao, HE Jin-tang, YU Ming-bo. Water retention behaviour of complete-intense weathering mudstone and its prediction[J]. Chinese Journal of Geotechnical Engineering, 2016, 38(z2): 216-221. DOI: 10.11779/CJGE2016S2035
Citation: NIU Geng, SUN De-an, WEI Chang-fu, YAN Rong-tao, HE Jin-tang, YU Ming-bo. Water retention behaviour of complete-intense weathering mudstone and its prediction[J]. Chinese Journal of Geotechnical Engineering, 2016, 38(z2): 216-221. DOI: 10.11779/CJGE2016S2035

Water retention behaviour of complete-intense weathering mudstone and its prediction

More Information
  • Received Date: May 18, 2016
  • Published Date: October 19, 2016
  • The pressure plate method, filter paper method, vapor equilibrium technique with saturated salt solution, transient water release and imbibition method and mercury intrusion porosimetry (MIP) tests are used to investigate the water retention behaviour and pore-size distribution of compacted complete-intense weathering mudstone specimens taken from Cenxi, Guangxi Province. Based on the results of the MIP tests experiencing two different suctions, a method for predicting the water retention curve is proposed. The test results show that the air entry value of complete-intense weathering mudstone is about 75 kPa, and the water retention curve in the full suction range can be measured by the three methods. There appears a plateau stage in SWCC. The SWCC calculated by TRIM matches the results of conventional tests. The saturated specimen exhibits a unimodal pore-size distribution, and the specimen experiencing suction of 38 MPa has a double-porosity microstructure. There are mainly intergranular pores with diameter of 102 nm to 103 nm in compacted samples of complete-intense weathering mudstone. With the increase of the suction, the pores in this diameter range decrease. The SWCCs fitted by Van Genuchte and Fredlund & Xing are more close to the measured results accurately, and those fitted by other models cannot match the measured water retention curve correctly in the full suction range.
  • [1]
    GB 5007—2011建筑地基基础设计规范[S]. 2011. (GB 5007—2011 Code for design of building foundation[S]. 2011. (in Chinese))
    [2]
    纪文奇, 费涵昌. 泥岩风化物的工程特性与应用[J].工程勘察, 1999, 7(2): 8-10. (JI Wen-qi, FEI Han-chang. Engineering characteristics and application of mudstone weathering[J]. Engineering Investigation, 1999, 7(2): 8-10. (in Chinese))
    [3]
    胡 冉, 陈益峰, 周创兵. 基于孔隙分布的变形土土水特征曲线模型[J]. 岩土工程学报, 2013, 35(8): 1451-1462. (HU Ran, CHEN Yi-feng, ZHOU Chuang-bing. A water retention curve model for deformable soils based on pore size[J]. Chinese Journal of Geotechnical Engineering, 2013, 35(8): 1451-1462. (in Chinese))
    [4]
    VANAPALLI S K, FREDLUND D, PUFAHL D E. The influence of soil structure and stress history on the soil-water characteristics of a compacted till[J]. Géotechnique, 1999, 49(2): 143-59.
    [5]
    陈正汉. 非饱和土与特殊土力学的基本理论研究[J].岩土工程学报, 2014, 36(2): 201-272. (CHEN Zheng-han. On basic theories of unsaturated soils and special soils[J]. Chinese Journal of Geotechnical Engineering, 2014, 36(2): 201-272. (in Chinese))
    [6]
    WAYLLACE A, LU Ning. ATransient water release and imbibitions method for rapidly measuring wetting and drying soil water retention and hydraulic conductivity functions[J]. Geotechnical Testing Journal, 2012, 35(1): 1-15.
    [7]
    VOGEL T, VAN GENUCHTEN M TH, CISLEROVA M. Effect of the shape of the soil hydraulic functions near saturation on variably-saturated flow predictions[J]. Advances in Water Resources, 2001, 24: 133-144.
    [8]
    LEIJ F J, RUSSELL W B, LESCH S M. Closed-form expressions for water retention and conductivity data[J]. Ground Water, 1997, 35(5): 848-858.
    [9]
    孙德安, 高 游. 不同制样方法非饱和土的持水特性研究[J]. 岩土工程学报, 2015, 37(1): 91-97. (SUN De-an, GAO You. Water retention behaviour of soils with different preparations[J]. Chinese Journal of Geotechnical Engineering, 2015, 37(1): 91-97. (in Chinese))
    [10]
    孙德安, 高 游, 刘文捷, 等. 红黏土的土水特性及其孔隙分布[J]. 岩土工程学报, 2015, 37(2): 351-355. (SUN De-an, GAO You, LIU Wen-jie, et al. Soil-water characteristics and pore-size distribution of lateritic clay[J]. Chinese Journal of Geotechnical Engineering, 2015, 37(2): 351-355. (in Chinese))
    [11]
    ROMERO E, VAUNAT J. Retention curve of deformable clays[C]// Proceedings International Workshop on Unsaturated Soils. Rotterdam: A A Balkema, 2000: 91-106.
    [12]
    ASTM Committee D 5298-03. Standard test method for measurement of soil potential (suction) using filter[S].
    [13]
    LEONG E C, HE L, RAHARDJO H. Factors affecting the filter paper method for total and matric suction measurements[J]. Geotechnical Testing Journal, 2002, 25(3): 1-12.
    [14]
    孙德安, 张俊然, 吕海波. 全吸力范围南阳膨胀土的土-水特征曲线[J]. 岩土力学, 2013, 33(8): 1839-1846. (SUN De-an, ZHANG Jun-ran, LU Hai-bo. Soil-water characteristic curve of Nanyang expansive soil in full suction range[J]. Rock and Soil Mechanics, 2013, 33(8): 1839-1846. (in Chinese))
    [15]
    OIMLR 121饱和盐溶液标准相对湿度值[S]. 2000. (OIMLR 121 The standard values of relative humidity for saturated salt solutions[S]. 2000. (in Chinese))
    [16]
    FREDLUND D G, XING A. Equations for the soil-water characteristic curve[J]. Canadian Geotechnical Journal, 1994, 31(3): 521-532.
    [17]
    WASHBURN E W. Note on a method of determining the distribution of pore sizes in a porous material[J]. Proceedings of the National Academy of Sciences of the United States of America, 1921, 7(4): 115-116.
    [18]
    KODIKARA J, BARBOUR S L, FREDLUND D G. Change in clay structure behaviour due to wetting and drying[C]// Proceedings of 8th Australian-Zealand Conference on Geomechanics. Hobart, 1999: 179-185.

Catalog

    Article views (429) PDF downloads (404) Cited by()
    Related

    /

    DownLoad:  Full-Size Img  PowerPoint
    Return
    Return